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Tracing Ashoka in Ujjain: What fresh dig at Vaishya Tekri ‘stupa’ can and cannot reveal | Explained News - The Indian Express
https://indianexpress.com/article/explained/explained-history/ashoka-ujjain-fresh-dig-vaishya-tekri-stupa-10842043/
https://indianexpress.com/article/explained/explained-history/ashoka-ujjain-fresh-dig-vaishya-tekri-stupa-10842043/
The Indian Express
Tracing Ashoka in Ujjain: What fresh dig at Vaishya Tekri ‘stupa’ can and cannot reveal
Madhya Pradesh has begun a push to excavate monuments linked to Mauryan-era emperor Ashoka, beginning with Vaishya Tekri. Here's what history reveals about a young prince's life — and love — in modern MP.
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Union of India v. Rohith Nathan (2026) — Supreme Court Settles the OBC Creamy Layer Salary Controversy Once and For All
https://nyayanishtha.com/article/union-of-india-v-rohith-nathan-2026-supreme-court-settles-the-obc-creamy-layer-salary-controversy-once-and-for-all
https://nyayanishtha.com/article/union-of-india-v-rohith-nathan-2026-supreme-court-settles-the-obc-creamy-layer-salary-controversy-once-and-for-all
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Industry_Definition_Labour_Law_CLAT_Notes.pdf
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define ‘industry’ under labour law: Inside SC’s split verdict,What was the 1978 Bangalore Water Supply Judgment
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moraine dam
is a natural barrier formed by glacial debris—like rock, gravel, and sediment—piled up at the side or terminus of a retreating glacier.
These natural mounds trap meltwater to create moraine-dammed lakes, which are common in high-mountain regions like the Himalayas and the Andes.
As a glacier retreats, it leaves behind a ridge of rocky debris (a moraine) that acts like a wall holding back accumulated meltwater
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Nepal_Floods_Himalayan_Vulnerability_Disaster_Mgmt_Notes-1.pdf
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Nepal Floods 2026
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What is Permafrost?
Permafrost is essentially any ground that stays frozen — 0 degree Celsius or lower — for at least two years straight.
These permanently frozen grounds are often found in Arctic regions such as Greenland, Alaska (the United States), Canada, Russia and Eastern Europe.
Permafrost is essentially any ground that stays frozen — 0 degree Celsius or lower — for at least two years straight.
These permanently frozen grounds are often found in Arctic regions such as Greenland, Alaska (the United States), Canada, Russia and Eastern Europe.
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